FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2113055163> ?p ?o ?g. }

• W2113055163 endingPage "133" @default.
• W2113055163 startingPage "119" @default.
• W2113055163 abstract "The Kuwei mafic intrusion, consisting of hornblende gabbro, gabbro, gabbro norite, and olivine norite, lies in the southern Altai Mountains, northern Xinjiang. A combined field, geochronological, and geochemical study of the Kuwei intrusion is reported here. This study provides the first reliable SHRIMP U‐Pb zircon dating results for the intrusion, and these yielded an age of $$47pm 1$$ Ma, which is the first documented report of Eocene magmatism in the region. The chondrite‐normalized rare earth element patterns for the Eocene intrusions are flat, and most of the incompatible elements are comparably depleted. Thus, geochemical data suggest that the Kuwei mafic intrusion was produced by partial melting of asthenospheric mantle that was slightly contaminated by lithospheric material. We interpret the 47‐Ma magmatism to result from asthenospheric mantle upwelling following the progressive India‐Eurasian collision. Although the Kuwei intrusion is laterally beyond the limit of Eocene deformation normally attributed to the India‐Asia collision, the timing of magmatism in the intrusion suggests that lateral extension may have initially affected a wider region than the area later thickened by convergence in the Tibetan Plateau. The Kuwei intrusion and other plutons likely related to it may have been emplaced into dilational jogs in fault systems activated by the India‐Asia collision. The emplacement depth is estimated to be ∼6 km, based on geobarometric determinations. Erosion was imperceptible before 25 Ma but has worn away an average of 0.024 cm of uplift every year since 25 Ma. The 6 km of exhumation since the late Oligocene is also attributed to far‐field effects of the India‐Asia collision." @default.
• W2113055163 created "2016-06-24" @default.
• W2113055163 creator A5003218655 @default.
• W2113055163 creator A5007876335 @default.
• W2113055163 creator A5041185785 @default.
• W2113055163 creator A5044298413 @default.
• W2113055163 creator A5048297380 @default.
• W2113055163 creator A5054277973 @default.
• W2113055163 creator A5077567100 @default.
• W2113055163 creator A5090517968 @default.
• W2113055163 date "2008-03-01" @default.
• W2113055163 modified "2023-09-24" @default.
• W2113055163 title "Geochronology and Geochemistry of the Kuwei Mafic Intrusion, Southern Margin of the Altai Mountains, Northern Xinjiang, Northwest China: Evidence for Distant Effects of the Indo‐Eurasia Collision" @default.
• W2113055163 cites W1964599463 @default.
• W2113055163 cites W1966292982 @default.
• W2113055163 cites W1968450376 @default.
• W2113055163 cites W1970439132 @default.
• W2113055163 cites W1982687831 @default.
• W2113055163 cites W1986335413 @default.
• W2113055163 cites W1994997277 @default.
• W2113055163 cites W1997953775 @default.
• W2113055163 cites W2002325302 @default.
• W2113055163 cites W2002976321 @default.
• W2113055163 cites W2011607179 @default.
• W2113055163 cites W2015259026 @default.
• W2113055163 cites W2026298033 @default.
• W2113055163 cites W2027862110 @default.
• W2113055163 cites W2028895756 @default.
• W2113055163 cites W2041210616 @default.
• W2113055163 cites W2041418871 @default.
• W2113055163 cites W2044377600 @default.
• W2113055163 cites W2046220982 @default.
• W2113055163 cites W2057208829 @default.
• W2113055163 cites W2057520249 @default.
• W2113055163 cites W2057897039 @default.
• W2113055163 cites W2063269424 @default.
• W2113055163 cites W2083507185 @default.
• W2113055163 cites W2088528371 @default.
• W2113055163 cites W2088744580 @default.
• W2113055163 cites W2088908478 @default.
• W2113055163 cites W2089096123 @default.
• W2113055163 cites W2089561399 @default.
• W2113055163 cites W2094620160 @default.
• W2113055163 cites W2095114818 @default.
• W2113055163 cites W2096021121 @default.
• W2113055163 cites W2102187859 @default.
• W2113055163 cites W2110706788 @default.
• W2113055163 cites W2115518283 @default.
• W2113055163 cites W2135565807 @default.
• W2113055163 cites W2138522501 @default.
• W2113055163 cites W2141045798 @default.
• W2113055163 cites W2141599763 @default.
• W2113055163 cites W2164062396 @default.
• W2113055163 cites W2167383526 @default.
• W2113055163 cites W2168011730 @default.
• W2113055163 cites W2975886582 @default.
• W2113055163 cites W2995482781 @default.
• W2113055163 cites W4249361818 @default.
• W2113055163 cites W4249864805 @default.
• W2113055163 doi "https://doi.org/10.1086/527457" @default.
• W2113055163 hasPublicationYear "2008" @default.
• W2113055163 type Work @default.
• W2113055163 sameAs 2113055163 @default.
• W2113055163 citedByCount "4" @default.
• W2113055163 countsByYear W21130551632014 @default.
• W2113055163 countsByYear W21130551632015 @default.
• W2113055163 crossrefType "journal-article" @default.
• W2113055163 hasAuthorship W2113055163A5003218655 @default.
• W2113055163 hasAuthorship W2113055163A5007876335 @default.
• W2113055163 hasAuthorship W2113055163A5041185785 @default.
• W2113055163 hasAuthorship W2113055163A5044298413 @default.
• W2113055163 hasAuthorship W2113055163A5048297380 @default.
• W2113055163 hasAuthorship W2113055163A5054277973 @default.
• W2113055163 hasAuthorship W2113055163A5077567100 @default.
• W2113055163 hasAuthorship W2113055163A5090517968 @default.
• W2113055163 hasConcept C127313418 @default.
• W2113055163 hasConcept C13495919 @default.
• W2113055163 hasConcept C147717901 @default.
• W2113055163 hasConcept C151730666 @default.
• W2113055163 hasConcept C161509811 @default.
• W2113055163 hasConcept C162973429 @default.
• W2113055163 hasConcept C167284885 @default.
• W2113055163 hasConcept C16942324 @default.
• W2113055163 hasConcept C17409809 @default.
• W2113055163 hasConcept C202746551 @default.
• W2113055163 hasConcept C2777110262 @default.
• W2113055163 hasConcept C2778849375 @default.
• W2113055163 hasConcept C2780981397 @default.
• W2113055163 hasConcept C46375708 @default.
• W2113055163 hasConcept C77928131 @default.
• W2113055163 hasConcept C79605941 @default.
• W2113055163 hasConceptScore W2113055163C127313418 @default.
• W2113055163 hasConceptScore W2113055163C13495919 @default.
• W2113055163 hasConceptScore W2113055163C147717901 @default.
• W2113055163 hasConceptScore W2113055163C151730666 @default.
• W2113055163 hasConceptScore W2113055163C161509811 @default.
• W2113055163 hasConceptScore W2113055163C162973429 @default.
• W2113055163 hasConceptScore W2113055163C167284885 @default.

• next